摘要
河北赤城青羊沟铅锌银矿床发育热液充填交代、条带、压碎、揉皱、脉状及交错脉状等各种组构。反映了该矿床经历了沉积变质、岩浆热液改造等多成因的特点。
The Qingyang Canal Pb-Zn-Ag deposit in Chicheng County Hebei bears various fabrics such as hydrothermal filling -replace.ctripe. rupture. pell -mell structure ,vein. crossed vein, which reflect that the deposite has undergone a process of polygenetic property of sedimentation - metamorphosis and magmatic hydrothermal reformation and etc.
关键词
铅锌矿床
银矿床
矿石组构
矿床成因
ore fabric
polygenetic deposit
genesis of deposit
Chicheng
